Huang et al. reply

F. Huang (), P. Chakraborty, C. C. Lundstrom, C. Holmden, J. J. G. Glessner, S. W. Kieffer and C. E. Lesher
Additional contact information
F. Huang: University of Illinois
P. Chakraborty: University of Illinois
C. C. Lundstrom: University of Illinois
C. Holmden: University of Saskatchewan
J. J. G. Glessner: University of California
S. W. Kieffer: University of Illinois
C. E. Lesher: University of California

Nature, 2011, vol. 472, issue 7341, E2-E3

Abstract: Abstract Replying to F. M. Richter Nature 472, 10.1038/nature09954 (2011) In our Letter1, we showed that the phenomenon of isotope fractionation in silicate melts by thermal diffusion, first reported in 1998 (ref. 2), can be characterised by a parameter ΔST that is independent of temperature and composition. (Here ΔST is the difference in the Soret coefficient, ST, between isotopes of a diffusing element.) Richter3 questioned this finding by plotting Mg isotope ratio versus temperature data (figure 1 in ref. 3) for a subset of experiments from figure 3f of ref. 1.

Date: 2011
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DOI: 10.1038/nature09955

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